BUSCADOR RECOLECTA

(A) Our findings suggest that TORC1 blocks Cbk1 kinase activity in the absence of Cdc15 function while cells are arrested in late anaphase at 37 °C, which would promote a defect in the following cell separation as secretory vesicle transporting hydrolases would be unable to fuse into the plasma membrane. (B) Rapamycin inhibits TORC1 and would induce the accumulation of a hypophosphorylated version of Cbk1 that would be able to phosphorylate its key substrates as the exocyct component Sec3, which regulates the function of the SNARE complex at the site of division to promote fusion of secretory vesicle at the plasma membrane. Hydrolases contained in secretory vesicle are released to promote cell separation., Peer reviewed

This dataset comprises 20 folders corresponding to the 10 iron plus 10 manganese IRIS film samplings in Salineta playa-lake. Each IRIS sampling includes also a video obtained with the clear IRIS tubes installed close to the IRIS films. We followed the method and camera instrument described in Scott et al. (2021) (DOI: 10.1002/saj2.20171). The videos of the soil allowed the direct monitoring of the oxide-paint removal and guided the successive sampling of the IRIS films. Each sampling included the video-image monitoring of the clear-IRIS tubes and the retrieval of three replicates of Fe and Mn IRIS films. Each folder contains the field photographs of the three iron or manganese films sampled. The photographs were processed: after cropping to the area of interest, they were binarized and the reduced (white) area of the film was then quantified. The numbering of the folders follows the order of sampling, from 1 to 10, and folders are labeled with F for iron and with M for manganese films. The Excel worksheet included in the present dataset contains the quantification data of the oxide-coating removed from iron and manganese films, together with the quantification of the black sulfides deposited on the iron films. The film area under reducing conditions (white PVC film) is expressed in percentage of the total film area. This percentage of paint removed has been calculated: 1) for every cm of the film depth (50 cm), 2) in the upper 0-30 cm of the film, and 3) in the total length of the film (0-50 cm). The removal rate indicates the reducing conditions evolution and intensity in the studied soils of the saline wetland., The data corresponds to the Spanish study area, the Salineta inland saline wetland (41°28'55.34"N, 0° 9'23.59"W) located 60 km far from Zaragoza city, in one of the most arid areas of the Central Ebro Basin, NE Spain. In this project we studied the redox conditions of the hypersaline soils in Salineta playa-lake, which are subjected to intermittent flooding, along a period of 17 months, in 2019 and 2020. The data were obtained during the monitoring of the soil redox conditions using IRIS (Indicators of Reduction in Soils) films and clear IRIS tubes coated with iron oxide and manganese oxide and supplied by the Prof. Martin Rabenhorst and Dr. Brian Scott, from the University of Maryland, USA. The monitoring of the IRIS films consisted on the quantification of the oxide-coating removed from the films. The oxide-coating of the films was reduced and then dissolved due to the microbial action. Firstly, the manganese-oxide coated films and later the iron-oxide coated films lost gradually their cover paint until showing the white underlying PVC film without paint., These data belong to the research project (AQUASALT), EraNET that in Spain has been supported by grant PCI2018-09299 funded by MCIN/AEI/10.13039/50110 0 011033 and co-funded by the European Union., Peer reviewed

1 .zip file containing aerial photographs (.pdf files)., Scans of paper contact copies of aerial photographs with the wax pencil marks by the soil surveyors in 1975. The survey area is the land irrigated by the Canal of Flumen at the left side of the River Flumen in the province of Huesca, Spain., Peer reviewed

We have organized the data in three files: • File "Augerings 1975 Monegros.docx", a list of the 519 soil samples taken by hand-auger in 1975 at 183 sites. The list shows the refernce of the sampling site, the depth of each sample, the electrical conductivity at 1:5 dilution, and the pH at 1:1 dilution; • File "Coordinates 1975 Monegros.docx", the UTM coordinates of the sampling sites; and • File "Marked contacts CETFA Monegros1972 and diagram.zip”, the scannings in pdf format of the 176 contacts aerial photographs from a flight of 1972 that have marks of the surveyors for the localization of the sampling sites. This zip file also contains the flight diagram in pdf format., Salinity is a time-variable characteristic trait of the soils, as is well known in the irrigated lands. Tracking the variation of soil salinity along time is a way to evaluate the effects of irrigation in agricultural lands or in their surroundings. Such evaluations can enable warning and even implementing corrective actions if salinity underwent undesirable evolution. The data presented here come from a heritage report commissioned by IRYDA, the organism in charge of new irrigation projets within the Spanish Ministry of Agriculture., The time elapsed and the changes in the irrigation techniques in the district, where now is becoming majoritarian the pressurized application of water, reinforce the interest of this dataset for multitemporal evaluations with agronomical or environmental purposes., Peer reviewed

Supplementary Fig. 1. Schematic representation of the peptide array. Supplementary Fig. 2. Screening of the antibodies present in the pre-immune bleed and in four post-immunization bleeds collected from a sheep immunized with HNE-modified HSA. Supplementary Fig. 3. SA369 anti-HSA-HNE pAb enriched pAb purification chromatograms from affinity purification using an HSA-HNE-coupled resin to recover the mixture of anti-HA and anti-HSA-HNE IgGs (A) and an HSA-coupled resin for depletion of anti-HSA antibodies (B). Supplementary Fig. 4. Chromatogram obtained from the purification of the IgGs from the crude sheep sera (SA369) with a protein G resin (A) and from the enrichment of anti-HNE antibodies using a KLH-HNE conjugated resin (B). Supplementary Figure 5. Purification of SA369 pAbs from the sheep bleed SA369 using a KLH-HNE covalently bound to a sepharose resin. Supplementary Figure 6. ELISA assay comparing the binding of the anti-HNE Abcam and the Anti-HSA-HNE SA369 antibodies to recombinant HSA expressed in Saccharomyces cerevisiae and standard HSA (the same HSA molecule used for immunization). Supplementary Table 1. List of the human serum albumin (UniProt ID: P02768) peptides synthesized on the arrays, Supplementary data for the article https://doi.org/10.1016/j.freeradbiomed.2019.05.008, Peer reviewed

Number and frequency of visits to Pyrus bourgaeana trees in southern Spain. The number of visits has been added to this file for first time., PID2022-142067NB-I00 CGL2017- 84633- P FPU17/04375, Peer reviewed

1 file, Database including the hydrographic and biogeochemical data collected along the A16N&S, within the GO-SHIP program in 2013. The database also includes the water mass proportions calculated using an OMP analysis. This is the database that was used in the paper "Net additions of recalcitrant dissolved organic carbon in the deep Atlantic Ocean", submitted to Global Biogeochemical Cycles, Peer reviewed

1 zip file, Optimum Multiparameter Model in Matlab code to solve the mixing of water masses in the North and South Atlantic ocean based on GOSHIP cruises with available Dissolved Organic Carbon (DOC) data. Data below 250 dbar and colder than 14ºC are considered. The scripts solve the mixing of central, intermediate, deep and bottom waters crossed by the GOSHIP lines (A22-2012, A20-2012, A13.5-2010, A16N-2013, A16S-2013). INPUT variables are the comprised within a matlab file (OMP_ATL_DOM.mat) containing hydrographic and biogeochemical data as provided in the OCADS repository for Repeat Hydrography. The OUTPUT is generated in the file OMP_RESULTS.xlsx containing self explaining names of the output variables. A detailed explanation of the OMP settings, constraints and results to analyse and check is given in the linked Global Biogeochemical Cycles manuscript. To inititate the OMP analysis just run "Megaprograma.m", the analysis will start and when ending the results will appear in the xlsx file, Peer reviewed

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3 files, Supporting information for the article https://doi.org/10.1074/jbc.RA118.004110, Peer reviewed